• 상하수도학회지
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• 제20권3호
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• pp.451-460
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• 2006

While sludge settles down in a batch column, sludge concentration becomes high. Sludge concentration change is one of the most critical causes of the sludge settling velocity variation. Therefore, sludge concentration change causes sludge index to change. SVI is more sensitive than other sludge indexes to the change of sludge concentration. And if sludge-water interface has reached final height within 30minutes, SVI is not suitable for prediction of sludge settling characteristic, Therefore, SVIs of each sludge are, in some cases, different although each sludge has the same settling velocity. But SVI has been widely used to interpret sludge settling characteristic by a simple testing method. This work has two purposes. The first purpose is to predict sludge settling velocity by using sludge-water interface settling velocity. And the second purpose is to develop new sludge settling characteristic index to exactly interpret sludge settling characteristic by overcoming the limit of SVI.

• 한국물환경학회지
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• 제23권6호
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• pp.807-813
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• 2007

Settling velocity is one of major parameters determining algal biomass in water quality modeling. In this study, the settling velocity of phytoplankton was measured in reservoir and stream sites of the Nakdong River, Korea. Settling velocities of various phytoplankton species were determined by measuring algal cell biomass settled in a sedimentation cylinder. Mean settling velocities were $0.22m\;day^{-1}$ in reservoir sites and $0.33m\;day^{-1}$ in stream sites, which were relatively higher compared with other default values suggested by water quality models (e.g. $0.1m\;day^{-1}$ in CE-QUAL-W2). The lower settling velocity in reservoirs than in stream implies the adaptation of phytoplakton to low turbulence in lentic environments. Cyanobacteria showed lower settling velocity ($0.2m\;day^{-1}$) than diatoms ($0.3m\;day^{-1}$), and this phenomenon may have resulted from buoyancy mechanisms of cyanobacteria. Cell volume did not show a significant correlation with settling velocity in this study, implying that conformation factors of colonies or other factors had large effects on settling velocity of algal cells as well as cell size. The result of this study may suggest proper coefficients of settling velocity of phytoplankton in the calibration of water quality model.

• 한국해양공학회지
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• 제12권2호통권28호
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• pp.111-120
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• 1998

Laboratory settling experiments (column, recirculating flume) were conducted for further understanding of the physical processes of cohesive sediment transport. \In still water experiments, the growth rate of flocculation is dependent upon the initial suspended concentration. Consequently, the settling velocity increases with concentration of flees. In flocculation settling regime, the exponent n in the settling velocity, $w_s=kC^n$, for Nakdong estuary mud was obtained empirically. The exponents were found to be 1.33, and 1.06 for the initial suspended concentrations of 1 g/i and 3 g/t, respectively. In flowing water, experiments for the median settling velocity with Nakdong mud in a recirculating flume were conducted. Settling velocity was found to depend much more strongly on the current velocity than initial concentrations. The temporal variation of suspended concentration increases as current velocity decreases.

• 상하수도학회지
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• 제20권1호
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• pp.156-163
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• 2006

While sludge is settling in batch column, sludge concentration becomes high. Because the characteristic of sludge settling changes in function of time due to the sludge concentration change, the sludge settling velocity changes too. Also, because the sludge settling characteristic is influenced by a physical characteristic of sludge and a column height etc, it is difficult to exactly measure the sludge settling characteristic. Although the sludge volume indexes, SVI, SSVI and $SSVI_{3.5}$, are used to predict sludge settling characteristic, these indexes are not reliable values. Because the previously established models for sludge settling velocity predict the sludge settling velocity only, it is difficult to predict sluge-water interface height by using those models. The purpose of this experiment is to establish the empirical model which predicts the sludge interface height change with respect to the sludge physical characteristic and the settling condition.

• 한국수자원학회논문집
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• 제40권9호
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• pp.723-734
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• 2007

본 연구는 점착성 퇴적물 예측에 가장 중요한 인자인 침강속도를 강 항만 저수지 그리고 호수에 녹아있는 이온 $(Na^+,\;Cl^-,\;OH^-,\;H^+)$의 첨가 및 밀도의 변화 아래 실시되었다. 정수 중에 부유된 미립자(alumina와 quartz)의 침강 속도는 압력센서(최대 10 mbar)로 측정되었다. 초기 농도 20 g/l에서 alumina와 quartz의 평균 침강속도는 미립자의 응집현상 때문에 최고 값을 보였으며, 이때 각각 최대 평균 침강속도는 0.185 mm/s(alumina)와 0.022 mm/s(quartz)이다. 그 후 증가된 초기농도일 경우 간섭침강 때문에 침강속도는 감소하였다. 또한 증가된 염분에서 두 미립자의 평균속도는 증가하였다. 더구나 alumina의 평균 침강속도는 산성에서 감소하다가 알칼리성에서는 강한 응집현상 때문에 높게 측정되었다. 그러나 quartz의 평균 침강속도는 알칼리성에서 낮은 값을 보였다.

• 상하수도학회지
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• 제20권1호
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• pp.147-155
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• 2006

For the further study of the solids flux theory, several researchers have proposed models to predict sludge settling velocity for each different concentration by using sludge indexes, SVI, SSVI and $SSVI_{3.5}$. It is difficult to apply the above models to predict sludge-water interface height in a batch column because sludge settling velocity changes while sludge settle down. While sludge settle down in a batch column, sludge concentration becomes high. The sludge concentration change is one of the most critical causes of the change of sludge settling velocity. Also, sludge concentration change causes of sludge index to change. SVI is more sensitive than SSVI or $SSVI_{3.5}$ to the change of sludge concentration. Each sludge has physical characteristics of its own which makes the settling velocity for each sludge different. The purpose of this study is to establish the correction factors that are able to compensate the errors derived from each different sludge settling characteristic by using sludge indexes, therefore the correction factors are applicable to the model for the change of sludge-water interface height.

• 한국지반환경공학회 논문집
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• 제16권10호
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• pp.33-38
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• 2015

본 논문에서는 물속에서의 조립입자 침강속도에 대한 특성을 파악하기 위해 다양한 재료 및 입자크기에 대한 실험적 관찰을 수행하고 그 결과들을 재료별로 비교함과 더불어 기존에 발표된 입자침강속도 예측을 위한 경험식들과 상호비교하였다. 본 연구에서는 폴리아세탈, 유리 및 스틸의 세 가지 서로 다른 재료 및 크기로 구성된 구모양의 입자를 이용하였으며, 입자의 직경은 1mm에서 20mm까지 다양한 직경을 고려하였다. 실험결과, 조립입자의 침강속도는 아주 작은 크기(약 $50{\mu}m$ 이하)의 입자에만 적용된다고 알려진 Stokes 식과는 상당한 차이를 나타냈으며, 또한 입자의 크기에 관계없이 침강속도를 예측하는 다른 연구자들의 경험식들과도 입자의 크기 및 재료의 종류(밀도)에 따라 서로 상이한 결과를 나타냈다. 실험에서 관찰된 조립입자의 침강속도는 재료의 종류에 관계없이 입자의 크기가 상대적으로 작을 때는(약 3mm 이하) 기존의 입자 침강속도에 대한 경험식들과 유사하였으나 그 이상에서는 입자의 크기가 증가할수록 기존 경험식들과의 차이도 더 크게 발생하였다. 본 연구를 통해서 조립입자의 침강속도는 입자의 크기 및 재료밀도에 따라 상당한 차이가 발생할 수 있다는 것을 알았으며 기존 경험식들은 실제로 발생하는 조립입자의 침강속도를 잘 예측하지 못해 향후 조립입자의 침강속도를 예측하기 위해 기존 경험식들을 있는 그대로 적용하지는 말아야 하고 실험 등을 통해 검증 및 확인하는 과정이 반드시 필요하다는 것을 파악하였다. 본 연구결과는 향후 물속에서의 조립입자의 침강속도를 이해하는 데 유용한 정보를 제공할 수 있을 것으로 판단된다.

• 한국해양공학회지
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• 제16권5호
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• pp.41-48
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• 2002

Numerical experiments are conducted using a three-dimensional baroclinic equation model and a Lagrangian method for clarifying the effect of th settling velocity on the suspended solids diffusion caused by the dredging and the reclamination works. Diffusion characteristics of the neutral particles and the weighting particles is experimented by the Lagrangian particles trajectory model, The results show that the diffusion characteristics of the suspended solids is effected by the settling velocity classified by the particles size in the density layered semi-closed bay. To estimate exactly the diffusion characteristics of the suspended solids and the contaminant with weight the three-dimensional baroclinic equation model and the three-dimensional Lagrangian particles trajectory model considering the settling velocity of the particle in the density layered semi-closed bay must be used.

• 한국해양공학회지
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• 제22권1호
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• pp.37-45
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• 2008

The purpose of this study is to quantify the settling velocities of cohesive sediments from Han estuary and to evaluate their local variation within Han estuary. This study also includes an estimation of their spatial variation, for which the settling velocities of cohesive sediments from Han estuary arecompared with those for sediments from other regions. At the same time, physical-chemical properties, such as grain size distribution, the percentage of organic contents, mineralogical composition etc are measured in this study in order to examine their correlation with settling velocities and their effect on settling velocities. Results from settling tests shaw that the settling velocities of Han estuary mud varies in the range of two orders of magnitude(from 0.01 to 1.5 mm/sec) over the corresponding concentration range of 0.1 to 80 g/L, and a feature of the settling velocity profile is quite different in quantity as compared to those of previous studies for muds from other regions. Particularly in the flocculated settling region, the settling velocity for Han estuary muds is shown to be larger than that of Saemankeum and Keum estuary sediments, while in the hindered settling region all three sediments are shown to have a similar settling velocity. However, local variability of the settling velocities within Han estuary is shown to be insignificant.

• 한국해양환경ㆍ에너지학회지
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• 제5권1호
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• pp.3-10
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• 2002

미세점착성 퇴적물 침강속도의 정량적 산정은 퇴적학적 측면에서뿐만 아니라 환경공학적 측면에서도 매우 중요한 과제이다. 미세점착성 퇴적물의 침강특성은 입자간의 충돌과 입자간의 점착으로 인하여 발생하는 응집에 의해 크게 영향을 받는다. 한편, 미세점착성 퇴적물의 응집강도는 광물질 구성, 입경분포, 유기물 함량 등으로 묘사되는 퇴적물의 물리ㆍ화학적 기본 특성에 따라 크게 변화하고, 이러한 물리ㆍ화학적 기본특성은 또한 지역적으로 변화하므로, 한 특정지역에서의 점착성 퇴적물의 침강특성은 현장관측이나 실내실험을 통하여 관측되어야만 한다. 본 연구에서는 최근 수행된 새만금 및 군산해역 점착성 퇴적물의 침강속도 관측 결과를 이용하여, 기존의 침강속도 경험식을 검토하고, 새로운 침강속도 곡선식이 개발된다. 새로 개발된 침강속도 곡선식은 기존의 복잡한 곡선식에 비해 단순하며, 측정치로부터의 계수산정이 편리하고, 또한 측정치의 변화 경향을 더욱 잘 나타낸다.